4.8 Review

The Chicxulub impact and its environmental consequences

Journal

NATURE REVIEWS EARTH & ENVIRONMENT
Volume 3, Issue 5, Pages 338-354

Publisher

SPRINGERNATURE
DOI: 10.1038/s43017-022-00283-y

Keywords

-

Funding

  1. NERC [NE/P005217/1]
  2. NSF-OCE [1736951]
  3. VeWA consortium (Past Warm Periods as Natural Analogues of our High-CO2 Climate Future) by the LOEWE programme of the Hessen Ministry of Higher Education, Research and the Arts, Germany
  4. Division Of Ocean Sciences
  5. Directorate For Geosciences [1736951] Funding Source: National Science Foundation

Ask authors/readers for more resources

This review explores how the Chicxulub impact structure provides insight into cratering processes and events leading to the Cretaceous-Palaeogene extinction.
The extinction of the dinosaurs and around three-quarters of all living species was almost certainly caused by a large asteroid impact 66 million years ago. Seismic data acquired across the impact site in Mexico have provided spectacular images of the approximately 200-kilometre-wide Chicxulub impact structure. In this Review, we show how studying the impact site at Chicxulub has advanced our understanding of formation of large craters and the environmental and palaeontological consequences of this impact. The Chicxulub crater's asymmetric shape and size suggest an oblique impact and an impact energy of about 10(23) joules, information that is important for quantifying the climatic effects of the impact. Several thousand gigatonnes of asteroidal and target material were ejected at velocities exceeding 5 kilometres per second, forming a fast-moving cloud that transported dust, soot and sulfate aerosols around the Earth within hours. These impact ejecta and soot from global wildfires blocked sunlight and caused global cooling, thus explaining the severity and abruptness of the mass extinction. However, it remains uncertain whether this impact winter lasted for many months or for more than a decade. Further combined palaeontological and proxy studies of expanded Cretaceous-Palaeogene transitions should further constrain the climatic response and the precise cause and selectivity of the extinction. The Chicxulub impact 66 million years ago caused catastrophic environmental changes, leading to the extinction of three-quarters of plant and animal species, including the dinosaurs. This Review explores how the Chicxulub impact structure provides insight into cratering processes and events leading to the Cretaceous-Palaeogene extinction.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.8
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available